首页> 外文会议>Biennial SGA meeting;Quadrennial IAGOD symposium >The deep causes of formation of the regional ore-forming system and ore zoning of the Le-De metallogenic belt, Jiangxi, China
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The deep causes of formation of the regional ore-forming system and ore zoning of the Le-De metallogenic belt, Jiangxi, China

机译:江西乐德成矿带区域成矿体系形成及成矿带深层成因

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The Le-De metallogenic belt is an important metallogenic district of base and precious metals in South China. Mineralizationoccurred most intensively during the Mesozoic Era and was closely related to andesitic igneous rocks formed from a syntectic magma derived from the mantle and crust. It constitutes an integrated regional ore-forming system and displays the following regional ore zoning: Cu-Au(Mo) -> Au -> Cu -Pb-Zn-Au-Ag -> Pb-Zn-Ag-Au ->Ag-Au. A deep-seated structure may be responsible for the formation of the ore-forming system and the ore zoning in the Le-De metallogenic belt.
机译:乐德成矿带是中国南方重要的贱金属和贵金属成矿区。成矿作用发生在中生代,是与地幔和地壳的共晶岩浆形成的安山岩火成岩密切相关的。它构成了一个集成的区域成矿系统,并显示以下区域矿石分区:Cu-Au(Mo)-> Au-> Cu -Pb-Zn-Au-Ag-> Pb-Zn-Ag-Au-> Ag-金深层结构可能负责成矿体系的形成和Le-De成矿带中的矿带。

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